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Published byFrancis Miller Modified over 9 years ago
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The Devil’s in the Details Transits in detail Telescopes
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Last time…. Radial velocity – Measures Doppler shift – Planet’s mass – Must be in line-of-sight of observer – Need a large telescope for high-precision measurements 1 m/s ~ 1 Earth-sized planet, need 6 m class telescope Transit – Measures drop in light as planet moves in front of or behind host star – Planet’s radius – Must be in line-of-sight of observer – Can do with a relatively small telescope
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Transit What is it measuring?
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Transit The atmosphere + the planet’s disk
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Transit The atmosphere + the planet’s optically-thick disk
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Transit The atmosphere + the planet’s optically-thick disk
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Transit Amount of atmospheric absorption will change with wavelength
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Transit Amount of atmospheric absorption will change with wavelength
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Transit So a planet’s radius will change with wavelength due to absorption by different molecules in its atmosphere
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So…. If we measure the transit of an exoplanet at different wavelengths… – We can measure how its radius varies with wavelength – Indicates its atmospheric structure and content Atmospheric structure = how temperature varies with altitude Atmospheric content = what molecules are present
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Example! Detection of H 2 scattering Zellem et al. (in prep.)
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Example! Detection of H 2 scattering
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Another Example! Detection of water, methane, and carbon dioxide in a hot Jupiter’s atmosphere Swain et al. (2009)
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Measuring radii at the 61” Planet has same signature in the infrared (IR) despite differing atmospheric contents optical Signal very different in the optical Benneke & Seager (2013)
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Why are the IR signatures the same? In the IR, a small planet with a thick atmosphere can block as much light as a large planet with a small atmosphere – Hot Jupiter atmospheres are opaque in the IR
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Why are the IR signatures the same? In the IR, a small planet with a thick atmosphere can block as much light as a large planet with a small atmosphere – Hot Jupiter atmospheres are opaque in the IR =
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However, not the same in the visible In the visible, the planet’s atmosphere is now transparent, so a small planet will look different than a large one
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However, not the same in the visible In the visible, the planet’s atmosphere is now transparent, so a small planet will look different than a large one ≠
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Rob does spectroscopy magic
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Measuring radii at the 61” Planet has same signature in the infrared (IR) despite differing atmospheric contents optical Signal very different in the optical Benneke & Seager (2013)
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Telescopes
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History First telescopes were refractors in the Netherlands in 1608 Galileo heard about them in 1609 and built his own – First person to point towards the heavens – Discovered craters on Moon, moons of Jupiter, Saturn’s rings
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Refractors vs. Reflectors Refractor: objective lens on front refracts (focuses) light at the back end of the telescope – Lens can obscure image – Very long focal length, so telescope itself is long
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Refractors vs. Reflectors Reflector: primary mirror reflects light to a focal point – No more lens – Can reflect the image back on itself, makes shorter focal length and telescope – Developed by Newton in 1680 Most professional telescopes today are reflectors Schmidt-Cassegrain design
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What is the 61”? Reflector or refractor?
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What is the 61”? Light comes in the dome, hits primary mirror
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What is the 61”? Reflected off of primary mirror and focused on secondary mirror
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What is the 61”? Light reflects off of secondary mirror and is focused on detector
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What is the 61”? REFLECTOR
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Next time…. Learn about instrumentation used to collect data – CCDs – Spectrographs Start learning how we will reduce telescopic data
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Calendar Next class: Friday October 24 Field trips! – Visit the 61” on Mount Bigelow Afternoon of Saturday November 1 Limited space for those who want to stick around through the night to help observe Will need people willing to help drive/carpool up the mountain – Mirror Lab Tour Friday November 14 from 4-5 PM
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